Inda Zib'i
Inda Zib'i is a reservoir located in the Inderta woreda of the Tigray Region in Ethiopia. The earthen dam that holds the reservoir was built in 1999 by SAERT.[1]
| Inda Zib'i | |
|---|---|
 | |
  Inda Zib'i | |
| Coordinates | 13.46980156°N 39.65274114°E |
| Type | Freshwater artificial lake |
| Basin countries | Ethiopia |
| Surface area | 0.04 km2 (0.015 sq mi) |
| Water volume | 0.182593×106 m3 (148.031 acre⋅ft) |
| Surface elevation | 2,400 m (7,900 ft) |
| Settlements | Araguren |
Dam characteristics
- Dam height: 12.34 metres
- Dam crest length: 227 metres
- Spillway width: 2 metres
Capacity
- Original capacity: 182 593 m³
- Dead storage: 20 000 m³
- Reservoir area: 4.05 ha
In 2002, the life expectancy of the reservoir (the duration before it is filled with sediment) was estimated at 25 years.[1]
Irrigation
- Designed irrigated area: 13 ha
- Actual irrigated area in 2002: 0 ha
Environment
The catchment of the reservoir is 1.49 km² large, with a perimeter of 4.77 km and a length of 1320 metres. The reservoir suffers from rapid siltation.[2][3] The lithology of the catchment is Agula Shale.[1] Part of the water that could be used for irrigation is lost through seepage; the positive side-effect is that this contributes to groundwater recharge.[4]
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References
- De Wit, Joke (2003). Stuwmeren in Tigray (Noord-Ethiopië): kenmerken, sedimentatie en sediment-bronnen. Unpub. M.Sc. thesis. Department of Geography, K.U.Leuven.
- Nigussie Haregeweyn, and colleagues (2006). "Reservoirs in Tigray: characteristics and sediment deposition problems". Land Degradation and Development. 17: 211–230. doi:10.1002/ldr.698.
- Vanmaercke, M. and colleagues (2019). "Sediment Yield and Reservoir Siltation in Tigray". Geo-trekking in Ethiopia's Tropical Mountains. GeoGuide. Cham (CH): Springer Nature. pp. 345–357. doi:10.1007/978-3-030-04955-3_23. ISBN 978-3-030-04954-6.
- Nigussie Haregeweyn, and colleagues (2008). "Sediment yield variability in Northern Ethiopia: A quantitative analysis of its controlling factors". Catena. 75: 65–76. doi:10.1016/j.catena.2008.04.011.
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